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Sedimentary stratigraphy of Eocene sheetflood deposits, Southern Pyrenees, Spain

Published online by Cambridge University Press:  01 May 2009

S. van der Meulen
S. van der Meulen
Affiliation:
Instituut voor Aardwetenschappen, Comparative Sedimentology Group, P.O. Box 80.021, 3508 TA Utrecht, The Netherlands
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Abstract

The Eocene Monllobat Formation of the southern Pyrenees accumulated under continental (non-marine) conditions. The total thickness of 180 m consists of seven cycles, defined by coarse member concentrations (often sheets) at the bases. The lateral extent of the sheets defines the fixed positions of eight parallel-trending alluvial systems, separated by narrow zones of fine sediment.

Sheetflooding dominated the sedimentation of these eight contemporaneous alluvial systems. The sediment was supplied from the rising axial zone of the Pyrenees. The cycles were caused by variations in tectonic activity. The positions and forms of coarse members were locally determined by contemporaneous faulting and folding of the alluvium.

Type
Articles
Information
Geological Magazine , Volume 123 , Issue 2 , March 1986 , pp. 167 - 183
Copyright
Copyright © Cambridge University Press 1986

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